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dc.contributor.authorGiménez, R.
dc.contributor.authorVilas, Lorenzo
dc.date.accessioned2020-06-26T09:30:48Z
dc.date.available2020-06-26T09:30:48Z
dc.date.issued1988
dc.identifier.urihttp://hdl.handle.net/10272/18392
dc.description.abstractDuring Late Cenomanian, an Atlantic transgression occurs as a result of the Iberian Plate tilting. Its southern limit is recognized in the Murcia-Albacete-Valencia area, with continental sediments, which are dividing the Iberian and Betic basins during that agees_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherTransgression boundaryes_ES
dc.subject.otherLate Cenomanianes_ES
dc.subject.otherIberian and Betic Rangeses_ES
dc.titleEl límite meridional de la transgresión cenomaniense superior en la Cordillera Ibérica (Murcia, Albacete y Valencia)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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